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Geology, U-Pb dating and 3D visualisation of late-orogenic Klenov Pluton (Pelhřimov Core Complex, Central European Variscides)

Author

Listed:
  • Jaroslava Pertoldová
  • Kryštof Verner
  • David Buriánek
  • Jan Valenta
  • Barbora Dudíková
  • Zuzana Skácelová
  • Jan Jelének
  • Jan Jelínek
  • Kenneth Johnson
  • Otmar Petyniak
  • Petra Hejtmánková

Abstract

The geological map of the Klenov Pluton (Moldanubian Batholith), and its 3D visualization, brings the new findings in the context of granite emplacement within late-Variscan settings. The Klenov Pluton has a peraluminous composition resulting from partial melting of metasedimentary sources and subsequent differentiation. The new ages 327.14 ± 0.21 Ma and 327.80 ± 0.37 Ma, reflect the narrow time-span of magma emplacement and cooling. The 327 Ma Klenov Pluton was emplaced syntectonically as a ‘sheet-like’ granite intrusion at depth ca. 10 kilometers during the later stages of the Pelhřimov Core Complex exhumation (at ca. 329 to 327 Ma) associated with ∼N–S oriented compression. Gravity modelling suggests that the Klenov Pluton has an asymmetric shape where its western flank is parallel to the ∼NW moderately dipping Pelhřimov Core Complex. The eastern margin of the Pluton is shallower and has been later modified by ∼SE-side-up normal faulting (Lodhéřov Fault Zone).

Suggested Citation

  • Jaroslava Pertoldová & Kryštof Verner & David Buriánek & Jan Valenta & Barbora Dudíková & Zuzana Skácelová & Jan Jelének & Jan Jelínek & Kenneth Johnson & Otmar Petyniak & Petra Hejtmánková, 2024. "Geology, U-Pb dating and 3D visualisation of late-orogenic Klenov Pluton (Pelhřimov Core Complex, Central European Variscides)," Journal of Maps, Taylor & Francis Journals, vol. 20(1), pages 2317144-231, December.
    • Handle: RePEc:taf:tjomxx:v:20:y:2024:i:1:p:2317144
    DOI: 10.1080/17445647.2024.2317144
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